 | John Wesley Judd - 1875 - 370 pagina’s
...France, and Western Germany, by the abundance of certain characteristic species (those of the Zone .if Ammonites Sowerbyi), local depression took place within...presenting many variations in its local characters, urn! constituting the formation to which we have applied the name "f the " Lincolnshire Oolite Limestone."... | |
 | William Jerome Harrison - 1882 - 406 pagina’s
...90 miles, the amount of depression being greatest in Central Lincolnshire. As a consequence of this, there was slowly accumulated, by the growth of coral...variations in its local characters, and constituting the formation to which we have applied the name of the "Lincolnshire Oolite Limestone." The western... | |
 | Adam and Charles Black (Firm) - 1884 - 326 pagina’s
...surface. Mr. Judd thus accounts for its formation: — "During a portion of the Jurassic period .... local depression took place within an area having...the action of marine currents sweeping small shells along the sea-bottom, a mass of calcareous strata, presenting many variations in its local characters,... | |
 | John Phillips - 1885 - 898 pagina’s
...period, within the life province or area now constituting Britain, Northern France, and Western Germany. Local depression took place within an area having...was slowly accumulated — by the growth of coral reufs, and the action of marine currents sweeping small shells and their fragments along the sea-bottom... | |
 | George Henry Burton - 1885 - 290 pagina’s
...miles, the amount of depression being greatest in ("entrai Lincolnshire. As a consequence of this, there was slowly accumulated, by the growth of coral...sweeping small shells and their fragments along the sea bottom, a mass of calcareous strata, presenting many variations in its local characters, and constituting... | |
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Sowerbyi), local depression took place within an area having a diameter of something like 90 miles, the amount of depression being greatest within its centre. As a consequence of this local depression there was slowly accumulated, by the growth of coral... 